Momudzhilgin Fm
Type Locality and Naming
Includes in East Pshart, East Pshart (southern slope), East Pshart (Agadjan river basin). It is identified in 1968 by V.I. Dranov.
Synonym: Momu Dzhilginskaya formation
Reference section:
Lithology and Thickness
90 m thick, is composed of gray debris-detrital limestones, clay slates, claystones, sandstones, and colorful cherts
Relationships and Distribution
Lower contact
conformably overlie the terrigenous suite, which relates to the Carboniferous - Ulyuk horizon of the lower division of the Permian (see the description of the Bazardarin Fm (базардаринской свиты).
Upper contact
Regional extent
They outcrop in the watershed and on the northern slope of the eastern part of the Shart Range.
GeoJSON
Fossils
In the limestones are enclosed foraminifera of the Kuberkandinsky horizon - Misellina sp., Cancellina sp., Armenina sp.; of the Murgab - Neoschwagerina haydeni Dutk., N. simplex Ozawa, etc., and of the Pamir horizon - Codonofusiella sp., Reichelina sp., Rauserella sp., etc. (determined by B.M. Gushin).
Age
Depositional setting
Additional Information